Brodtkorbite is an extremely rare copper-mercury selenide mineral first identified in the Skrikerum mining district of Sweden. It typically occurs as minute, metallic grains associated with other selenide minerals in hydrothermal deposits. Due to its extreme rarity and complex chemical composition, it is a significant specialty mineral for advanced systematic collectors.
Is this brodtkorbite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch brodtkorbite with a known reference. Brodtkorbite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: dark gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: dark gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, anhedral grains.
Often confused with
Brodtkorbite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside brodtkorbite
Minerals reported to co-occur with brodtkorbite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂HgSe₂
- Mohs hardness
- 2.5-3
- Density
- 7.77 g/cm³
- Colors
- Streak
- Dark gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, anhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Uncommon in telethermal selenium-rich hydrothermal polymetallic deposits, in calcite veins in amphibolites, formed below 112 °C
Where rockhounds find brodtkorbite
Classic worldwide localities
- Tuminico, Sierra de Cacho, La Rioja Province, Argentina (type locality)
- Příbram uranium and base-metal ore district, central Bohemia, Czech Republic
Field-hunting tip
Where it forms: Uncommon in telethermal selenium-rich hydrothermal polymetallic deposits, in calcite veins in amphibolites, formed below 112 °C. If you start seeing berzelianite, tiemannite, umangite in float, you are in the right ground. Typical habit: aggregates, anhedral grains. Train your eye for that shape before scanning the outcrop.






